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2020
Coupled atmosphere-ocean models are at the core of numerical climate models. There is an extraordinarily broad class of coupled atmosphere-ocean models ranging from sets of equations that can be solved analytically to highly detailed representations of Nature requiring the most advanced computers for execution.
Mechoso, C.R., An, S-Ii., Valcke, S.
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Coupled atmosphere-ocean models are at the core of numerical climate models. There is an extraordinarily broad class of coupled atmosphere-ocean models ranging from sets of equations that can be solved analytically to highly detailed representations of Nature requiring the most advanced computers for execution.
Mechoso, C.R., An, S-Ii., Valcke, S.
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Modeling Equatorial Ocean Circulation
Annual Review of Fluid Mechanics, 1985Double objectif de l'article: presenter, aussi succinctement que possible, les principes de la dynamique equatoriale, et passer en revue les recents developpements en la matiere. Les differents chapitres traitent successivement: des modeles suivant leur sophistication dynamique; des solutions non forcees, des solutions forcees par des vents qui s ...
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SPIE Proceedings, 2003
Remote sensing algorithms for retrieving estimates of oceanic constituent concentrations, such as chlorophyll concentration, require as input measurements of spectral water-leaving radiance. This measurement is typically obtained from space-based sensors such as SeaWiFS or MODIS.
Peter R. C. S. Fearns, Mervyn J. Lynch
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Remote sensing algorithms for retrieving estimates of oceanic constituent concentrations, such as chlorophyll concentration, require as input measurements of spectral water-leaving radiance. This measurement is typically obtained from space-based sensors such as SeaWiFS or MODIS.
Peter R. C. S. Fearns, Mervyn J. Lynch
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Models of the Ocean: Which Ocean?
2006Physics actually represented in an ocean model depend on each model’s resolution and its parameterization of subgridscale effects. This chapter is a review of parameterizations used in ocean models, focussing on operational ocean forecasting systems for the North Atlantic and Mediterranean Sea. This review is limited to z-coordinate models.
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Applied Acoustics, 1989
Abstract Four approaches to underwater sound propagation modelling are reviewed including rays, normal modes, Green's function integral, and parabolic equation. Specific programs are discussed. Particular reference is made to the problems in running models and the applicability in various regimes, especially deep-water environments.
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Abstract Four approaches to underwater sound propagation modelling are reviewed including rays, normal modes, Green's function integral, and parabolic equation. Specific programs are discussed. Particular reference is made to the problems in running models and the applicability in various regimes, especially deep-water environments.
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Bistatic model of ocean scattering
IEEE Transactions on Antennas and Propagation, 1998An analytical closed-form model is derived for the average power echo received by a bistatic altimeter from an oceanic surface at a frequency high enough for the Kirchhoff scattering mechanism to be dominant over the Bragg resonance one. The asymmetric behavior of the sea waves is taken into account, modeling the surface height as a non-Gaussian ...
PICARDI, Giovanni +3 more
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1985
Publisher Summary This chapter describes various aspects of the modeling of ocean circulation. Modeling the ocean circulation is entering a new era due to two major technical developments. One of these developments is the satellite-borne altimeter, which can provide a nearly synoptic view of the sea-surface elevation of the World Ocean.
Kirk Bryan, Jorge L. Sarmiento
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Publisher Summary This chapter describes various aspects of the modeling of ocean circulation. Modeling the ocean circulation is entering a new era due to two major technical developments. One of these developments is the satellite-borne altimeter, which can provide a nearly synoptic view of the sea-surface elevation of the World Ocean.
Kirk Bryan, Jorge L. Sarmiento
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Modelling ice-shelf/ocean interaction
2023The effect of climate change on the mass balance of ice shelves and bottom water formation is investigated using a terrain-following three-dimensional numerical ocean model. The Regional Ocean Modeling System was modified to simulate the thermodynamic processes beneath ice shelves, including direct basal processes and frazil ice dynamics.
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